New Caledonia vs Sri Lanka: Closed shrubland — Burning crop residues
New Caledonia
0 t
in 2024
Sri Lanka
0 t
in 2024
New Caledonia rank
34th
Sri Lanka rank
34th
Closed shrubland — Burning crop residues over time
- New Caledonia
- Sri Lanka
How they compare
New Caledonia currently reports 0 t against 0 t in Sri Lanka, a difference of 0 t.
The two have swapped places 6 times across 35 shared years of data; in 1990 it was Sri Lanka ahead.
New Caledonia ranks 34th and Sri Lanka ranks 34th of 219 countries.
Across the 4 decades both report, New Caledonia averaged higher in 2 and Sri Lanka in 2.
Head to head by decade
| Decade | New Caledonia | Sri Lanka | Difference | Ahead |
|---|---|---|---|---|
| 1990s | 591.56 t | 7,331 t | 6,740 t | Sri Lanka |
| 2000s | 457.21 t | 1,134 t | 676.76 t | Sri Lanka |
| 2010s | 171.5 t | 0 t | 171.5 t | New Caledonia |
| 2020s | 114.31 t | 0 t | 114.31 t | New Caledonia |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher closed shrubland — burning crop residues, New Caledonia or Sri Lanka?
- New Caledonia, at 0 t against 0 t in Sri Lanka as of 2024.
- What is the difference in closed shrubland — burning crop residues between New Caledonia and Sri Lanka?
- 0 t, with New Caledonia ahead.
- How many years of comparable data are there for New Caledonia and Sri Lanka?
- 35 years are reported by both, from 1990 to 2024.
- How do New Caledonia and Sri Lanka rank globally for closed shrubland — burning crop residues?
- New Caledonia ranks 34th and Sri Lanka ranks 34th of 219 countries.
- Where does this data come from?
- Food and Agriculture Organization of the United Nations, published as Closed shrubland — Burning crop residues (Biomass burned, dry matter). Statizoid refreshes it automatically from the source and publishes the full history for both places.
Individual pages
About this data
The FAOSTAT domain on Emissions from Fires consists of estimates of methane (CH4), nitrous oxide (N2O) and carbon dioxide (CO2) emissions generated from biomass burning in a range of vegetation types and from fires in organic soils.